Identification of Uterine Ion Transporters for Mineralisation Precursors of the Avian Eggshell Vincent Jonchère, Aurélien Brionne, Joël Gautron and Yves Nys*
Total Page:16
File Type:pdf, Size:1020Kb
Jonchère et al. BMC Physiology 2012, 12:10 http://www.biomedcentral.com/1472-6793/12/10 RESEARCH ARTICLE Open Access Identification of uterine ion transporters for mineralisation precursors of the avian eggshell Vincent Jonchère, Aurélien Brionne, Joël Gautron and Yves Nys* Abstract Background: In Gallus gallus, eggshell formation takes place daily in the hen uterus and requires large amounts of 2+ - the ionic precursors for calcium carbonate (CaCO3). Both elements (Ca , HCO3) are supplied by the blood via trans-epithelial transport. Our aims were to identify genes coding for ion transporters that are upregulated in the uterine portion of the oviduct during eggshell calcification, compared to other tissues and other physiological states, and incorporate these proteins into a general model for mineral transfer across the tubular gland cells during eggshell formation. Results: A total of 37 candidate ion transport genes were selected from our database of overexpressed uterine genes associated with eggshell calcification, and by analogy with mammalian transporters. Their uterine expression was compared by qRTPCR in the presence and absence of eggshell formation, and with relative expression levels in 2+ - 2+ - magnum (low Ca /HCO3 movement) and duodenum (high rates of Ca /HCO3 trans-epithelial transfer). We identified overexpression of eleven genes related to calcium movement: the TRPV6 Ca2+ channel (basolateral uptake of Ca2+), 28 kDa calbindin (intracellular Ca2+ buffering), the endoplasmic reticulum type 2 and 3 Ca2+ pumps (ER uptake), and the inositol trisphosphate receptors type 1, 2 and 3 (ER release). Ca2+ movement across the apical membrane likely involves membrane Ca2+ pumps and Ca2+/Na+ exchangers. Our data suggests that Na+ transport involved the SCNN1 channel and the Na+/Ca2+ exchangers SLC8A1, 3 for cell uptake, the Na+/K+ ATPase for cell output. K+ uptake resulted from the Na+/K+ ATPase, and its output from the K+ channels (KCNJ2, 15, 16 and KCNMA1). - - We propose that the HCO3 is mainly produced from CO2 by the carbonic anhydrase 2 (CA2) and that HCO3 is - - - 2+ + secreted through the HCO3/Cl exchanger SLC26A9. HCO3 synthesis and precipitation with Ca produce two H . Protons are absorbed via the membrane’sCa2+ pumps ATP2B1, 2 in the apical membrane and the vacuolar - - - (H+)-atpases at the basolateral level. Our model incorporate Cl ions which are absorbed by the HCO3/Cl exchanger SLC26A9 and by Cl- channels (CLCN2, CFTR) and might be extruded by Cl-/H+ exchanger (CLCN5), but also by Na+ K+ 2Cl- and K+ Cl- cotransporters. Conclusions: Our Gallus gallus uterine model proposes a large list of ion transfer proteins supplying Ca2+ and - HCO3 and maintaining cellular ionic homeostasis. This avian model should contribute towards understanding the mechanisms and regulation for ionic precursors of CaCO3, and provide insight in other species where epithelia transport large amount of calcium or bicarbonate. Keywords: Ion, Mineral, Calcium, Transporter, Uterus, Eggshell, Chicken * Correspondence: [email protected] INRA, UR83 Recherches Avicoles, F-37380, Nouzilly, France © 2012 Jonchère et al.; licensee BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Jonchère et al. BMC Physiology 2012, 12:10 Page 2 of 17 http://www.biomedcentral.com/1472-6793/12/10 Background uterine calbindin levels and Ca2+ flux [11,13,14]. This Biomineralisation is a process by which living organisms protein could also take part in maintaining low intracel- develop mineral structures to perform a variety of roles lular Ca2+ to avoid cell death as observed in other spe- related to support, defence and feeding. Amongst these, cies and tissues [15]. Ca2+ secretion from epithelial cells a large number of animals (birds, molluscs, foraminifera, to the uterine fluid is active involving a Ca2+ ATPase, corals, sea urchins) mineralises by co-precipitation of the activity of which varies with the stage of eggshell cal- 2+ 2- calcium (Ca ) and carbonates (CO3 ) to form a protect- cification [4,7]. A recent study [16] identified and loca- ive shell or a skeleton. The prerequisite for shell min- lized the plasma membrane Ca2+ ATPase isoform 4 eralisation is the supply of large amounts of Ca2+ and (PMCA4) in the apical membrane of epithelial cells of 2- + CO3 in a limited extracellular milieu by trans-cellular king quail. The disruption of sodium (Na ) re- transport, requiring the presence of ion channels, ion absorption by specific inhibitors in perfused uterus or pumps and ion exchangers. In Gallus gallus, eggshell in vitro reduced Ca2+ secretion by 50% [9,17], revealing formation takes place daily in the hen uterus and is one a strong relationship between Na+ and Ca2+ transfers of the most rapid mineralisation processes [1]. It and therefore the putative presence of Na+/Ca2+ exchan- + + requires large amount of calcium carbonate (CaCO3)as gers in uterine cells. The Na /K ATPase responsible for the hen exports the equivalent of her body weight as Na+ re-absorption in the plasma membrane is charac- eggshell in one year of egg production (>1.5 kg). Both terised and is upregulated during the period of shell 2+ - elements (Ca and HCO3) are not stored in the uterus calcification [18]. but are continuously supplied during eggshell formation The second essential component of eggshell mineral- by the blood plasma via trans-epithelial transport taking isation is carbonate. Blood carbon dioxide (CO2) is pro- place across the uterine glandular cells [2-4]. Early stud- vided in cells by passive diffusion through the plasma ies determined the ion concentrations of the uterine membrane [2,19]. In the uterine tubular gland cells, a fluid, which bathes the eggshell and changes during the family of key enzymes, the carbonic anhydrases (CA) [6] - sequential stages of calcification (Table 1) [5], identified catalyses the hydration of CO2 to HCO3 as confirmed by - several proteins involved in ion transport [3,6,7], and inhibition of HCO3production and secretion by acetazo- recorded changes in ion fluxes across the uterine epithe- lamide, a CA inhibitor [9]. Chloride (Cl-) is absorbed by lium in response to ion transporter inhibitors [8-10]. the uterus and any perturbation of Na+ flux by ouabain These classic approaches led to a hypothesis concerning [9] reverses both the Na+ and Cl- fluxes, but reduces also - the mechanisms of ion transfer through the uterine glan- HCO3 secretion suggesting that its transfer is dependent 2+ - - - dular cells (Figure 1; [1]). In hens, the Ca blood on Cl via a Cl /HCO3 exchanger which has not been -4 - (1.2 mM) and epithelial cell concentrations (10 mM), identified. Finally, the production of HCO3 in tubular 2+ 2+ 2- suggest that Ca entry in cell is passive via a Ca chan- gland cells and of CO3 in the uterine fluid generates nel, which remains unidentified. The intracellular Ca2+ high levels of protons (H+) ions. The concomitant de- transport through the cell involves 28 kDa calbindin crease in uterine and plasma pH during calcification [3,11,12]. The 28 kDa calbindin expression is greatly reflects the reabsorption of H+ [5]. upregulated during eggshell formation and falls after Only a few genes and related proteins involved in uter- suppression of calcification (by premature egg expul- ine ion transfer have been identified to date. Our object- sion), suggesting a very close relationship between ive therefore was to use the recent information issuing from the chicken genome sequencing [20] and subse- Table 1 PH and ion concentrations in blood plasma, quent enrichment in the chicken gene/protein databases uterine fluid and epithelial cells during eggshell to identify uterine ion transport proteins. Use of a recent mineralisation[5] transcriptomic study revealing uterine genes related to Blood plasma Epithelial cells Uterine fluid eggshell calcification [21] and of the analogies with 8 h PO 18 h PO transporters previously described in mammalian tissues Ions [mM] [mM] [mM] [mM] transferring large quantities of ions (intestine, kidney, Ca2+ 1.2 <0.0002 6 10 pancreas) allows the identification of putative genes en- Na+ 140 12 144 80 coding proteins involved in uterine trans-epithelial ion K+ 4 139 12 60 transports. Confirmation of their presence in birds and - evaluation of their involvement have been analysed by HCO3 23 12 60 110 comparing gene expression in the uterus compared to pH 7.4 7.0-7.4 7.6 7.1 the magnum (the oviduct segment responsible for the Cl- 130 4 71 45 synthesis and secretion of egg white proteins) and the The eggshell precursors are secreted in the uterine fluid where the eggshell 2+ mineralization daily takes place from 10 hours to 22 hours post ovulation (yolk duodenum (Ca uptake and neutralization of stomach 2+ - entry in the oviduct). PO: post ovulation. acid), where both Ca and HCO3 trans-epithelial Jonchère et al. BMC Physiology 2012, 12:10 Page 3 of 17 http://www.biomedcentral.com/1472-6793/12/10 Figure 1 Classic hypothesis concerning ion transfers in the hen uterus during eggshell calcification [1,5,8-10]. Ca2+ entry in cell is passive via a Ca2+ channel, 28 kDa calbindin contributes to intracellular transfer and maintenance of a low Ca2+ level. Ca2+ secretion involving a Ca2+ 2+ + ATPase and a Ca /Na exchanger. Carbonic anhydrase has a key role in providing carbonate from plasma CO2. transfers are respectively low and high. The magnum to the magnum (egg white protein secretion) [21] and and the uterus secrete a large amount of water, Na+ and analogies with transporters previously described in Cl- during the phase of hydration of egg albumen which mammalian tissues at the intestinal and kidney level takes place before the active phase of eggshell formation [24,26].